A separate chamber drains off the nastier parts of the brew.
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He drains off the buttermilk and then hand squeezes great lumps of it.
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The curds have set like a blancmange and as he cuts into them he frees up the whey, which drains off and out of the bath in streaky milky streams.
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The mould is usually a wire mesh that acts as a strainer such that the furnish is separated out of the water. The water drains off, leaving layers upon layers of fibers or a web of paper on the mould. The texture of the paper is determined by the nature of the mould.
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Sværsvann is a lake in the southeast of Oslo, Norway. The lake drains off into the river Hobølelva. The lake's surrounding areas are mostly residential. Sværsvann is a popular bathing place, and the name is believed to origin from "Sværd Vandet", which means "Sword Water", because a sword was once found at the bottom of the lake.
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The Chand Khali Nadi flows through the Patiya Plains, and the Dolukhal River drains into the Satkania Plains. Another tributary is the Kumira Khali, which drains into the Kutubdia Channel. There are seven Bangladesh Water Management Board hydrometric stations on this river, which have been recording data since 1965. The Sangu drains off the waters of Patiya, Satkania, and Banshkhali Upazilas.
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The Betwa drains off of the Deccan plateau. Originating in the Kumra village in Raisen district of Madhya Pradesh, the Betwa flows for 590 km (232 km in MP and 358 km in UP). After meandering through Madhya Pradesh, it enters the neighbouring state, Uttar Pradesh, and joins the river Yamuna (Jamna) in Hamirpur. The Betwa takes along with it the waters of the eastern Malwa plateau.
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The whole of the river drains off igneous and ancient rocks of the Cambrian and Ordovician which are all base-poor. Much of the catchment has also been used for commercial forestry during the last hundred years. As a consequence, many of the tributaries are highly acidic as a result of atmospheric acidification. This has constrained the quality of the fishery and the biodiversity in many tributaries.
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The heavy cold air that collects between the high peaks during the night drains off the heights much like water, joining cold moist air from the Santa Margarita River Channel to meander through the Temecula Valley, creating a double cooling effect. As a result, nighttime lows in and around Temecula are very cool. The cool nighttime temperatures are critical in developing high-quality grapes. Temecula Valley soils are another significant influence on wine quality.
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Without the computer to cycle the drains off, the spacecraft remained in a continuous negative net power configuration which eventually drained the batteries. When the battery voltage dropped below 8 V, the electronic switches for the drains defaulted to off, returning the spacecraft to positive net power and allowing the batteries to recharge. 7 September 2007: Once the batteries recharged sufficiently, the computer restarted successfully. Restart occurred 48 hours after the initial event.
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The replies given included gazettement could only be made once the Federal Lands and Mines Department had received all land titles from the Commissioner of Land. "Inside the fence" there is a small network of tarmac trails painted red and yellow and with poorly designed gutters that funnel the heavy rains into the middle of the road instead of into the drains. Off the tarmac in many directions are numerous mountain bike and walking trails that are maintained by dozens of local volunteers.
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Faraday used a gold-leaf electroscope, but modern demonstrations often use a modern electrometer because it is far more sensitive than an electroscope, can distinguish between positive and negative charge, and gives a quantitative readout., p.4-5 The container is discharged by connecting it briefly to a large conducting object, called a ground (earth); this can be done by touching it with a finger, using the conductive human body as a ground. Any initial charge drains off into the ground.
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After a major reconstruction, performed during the mid-seventies of the twentieth century, the drainage was drastically improved. The region of the Vierendeel is combined with the area south of Bedum and now drains off through the Harm Westerskanaal and the pumping station Casper Hommes on the Boterdiep just north of Zuidwolde. At the moment only the part between the railway-route Bedum - Stedum (there is a culvert here) and the Harm Westerskanaal is called the Kardingermaar. The other parts all have different drain directions, and thus are considered separate waterways.
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Folsom Dam spilling during a flood The American River Division is located in north-central California, on the east side of the Great Central Valley. Its structures use the water of the American River, which drains off the Sierra Nevada and flows into the Sacramento River. The division is further divided into three units: the Folsom, Sly Park and Auburn-Folsom South. The American River Division stores water in the American River watershed, to both provide water supply for local settlements, and supply it to the rest of the system.
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Mount Alfred is a mountain located at the Queen Reach arm and head of the Jervis Inlet within the Pacific Ranges of the Coast Mountains in British Columbia, Canada. The mountain is the highest in the portion of the mainland between Jervis and Toba Inlets, with its prominence defined by the pass at the head of the Skwawka River, which feeds the head of Jervis Inlet. The unofficially-named Alfred Creek Falls, on Alfred Creek which drains off the mountain's glaciers southeast into the Skwawka, is one of Canada's highest waterfalls at .
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Ice fields are formed by a large accumulation of snow which, through years of compression and freezing, turns into ice. Due to ice's susceptibility to gravity, ice fields usually form over large areas that are basins or atop plateaus, thus allowing a continuum of ice to form over the landscape uninterrupted by glacial channels. Glaciers often form on the edges of ice fields, serving as gravity-propelled drains off the ice field which is in turn replenished by snowfall. While an ice cap is not constrained by topography, an ice field is.
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Kelsey Bench shares both the valley and the TTB's AVA ruling with the Big Valley District AVA to the north. The region's growers submitted the two petitions together, drawing a line between the valley floor and the higher elevations in the south. The higher elevations of Kelsey Bench mean that the climate here is warmer than in Big Valley District, although not so warm as Red Hills Lake County in the east. Cold air from the mountains drains off the benches into the valley below, extending the growing season by lessening the risk of frost in the early spring and fall.
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By reducing soil erosion, cover crops often also reduce both the rate and quantity of water that drains off the field, which would normally pose environmental risks to waterways and ecosystems downstream. Cover crop biomass acts as a physical barrier between rainfall and the soil surface, allowing raindrops to steadily trickle down through the soil profile. Also, as stated above, cover crop root growth results in the formation of soil pores, which in addition to enhancing soil macrofauna habitat provides pathways for water to filter through the soil profile rather than draining off the field as surface flow. With increased water infiltration, the potential for soil water storage and the recharging of aquifers can be improved.
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An alternate way of conducting the experiment: after the charged object C is lowered into the container in Procedure 2, the outside surface of the container is momentarily grounded. The charge on the outside of the container all drains off to ground, and the charge detector declines to zero, leaving the charge on the inside of the container, equal but opposite to that on C. Then the object C is removed from the container. Since C is no longer present to hold the induced charge on the inside surface of the container, it migrates to the outside of the container. so the charge detector registers an equal but opposite charge from its previous reading.
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The land is made up of Wianamatta Shale, which heavily influences the soils and vegetation on reserve and is characterised by shallow to reasonably deep soils, including red and brown podzolic soils on the peaks, and yellow podzolic soils on lower slopes and in drainage lines. There is a small pocket of cleared land, that drains off- catchment within the north-eastern boundary of the Nature Reserve.Bannerman S M and Hazleton P A (1990) Soil Landscapes of the Penrith 1:100 000 Sheet, Soil Conservation Service of NSW, Sydney On the western slopes of George Maunder Lookout lies the Prospect dolerite intrusion, which is Sydney's largest body of igneous rock, that formed in the Early Jurassic after a volcanic activity where hot magmatic fluids moved through developing pegmatite and depositing prehnite, calcite and other secondary minerals found in the upper part of the intrusion. The eroded residue of the volcanic core forms the hill (or the laccolith) that is the George Maunder Lookout (and as well as the rest of Prospect Hill just the west of the Reserve), which was battered down over millions of years to a small jut in the generally flat lands of western Sydney.
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